Remote estimation of the diffuse attenuation coefficient in a moderately turbid estuary
Remote Sensing of Environment
By: R. P. Stumpf and J.R. Pennock
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Abstract
Solutions of the radiative transfer equation are used to derive relationships of water reflectance to the diffuse attenuation coefficient (K) in moderately turbid water (K > 0.5 m-1). Data sets collected from the NOAA AVHRR and in situ observations from five different dates confirm the appropriateness of these relationships, in particular the logistic equation. Values of K calculated from the reflectance data agree to within 60% of the observed values, although the reflectance derived using a more comprehensive aerosol correction is sensitive to chlorophyll concentrations greater than 50 ??g L-1. Agreement between in situ and remote observations improves as the time interval between samples is narrowed. ?? 1991.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Remote estimation of the diffuse attenuation coefficient in a moderately turbid estuary |
| Series title | Remote Sensing of Environment |
| Volume | 38 |
| Issue | 3 |
| Year Published | 1991 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Remote Sensing of Environment |
| First page | 183 |
| Last page | 191 |
| Google Analytic Metrics | Metrics page |